 
  
  
   
The LCC is a southwestward current following along the Russian coast. It
bifurcates into two branches near the east Russian bight (134 E,
42
E,
42 N): the western branch flows along the Russian-Korean coast and
becomes the NKCC. The eastern branch flows southeastward, then turns eastward
at 41.5
N): the western branch flows along the Russian-Korean coast and
becomes the NKCC. The eastern branch flows southeastward, then turns eastward
at 41.5 N, and becomes the south flank of the JB gyre. The LCC has a
strong seasonal variation with the maximum speed in the winter (Fig. 3a) and
the minimum speed in the summer (Fig. 3c).
N, and becomes the south flank of the JB gyre. The LCC has a
strong seasonal variation with the maximum speed in the winter (Fig. 3a) and
the minimum speed in the summer (Fig. 3c).